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NARRATOR: Planet Earth, four and a half billion years ago.
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A blazing sphere formed by colliding cosmic matter...
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a violent world, covered by a sea of molten lava.
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Over time, the surface cooled into a rocky crust.
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Great clouds of water vapor rose...
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then rained down, forming a vast ocean.
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The crust fractured into huge, moving plates
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that shifted the emerging continents...
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producing the face
of the planet we know.
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But the forces that created Earth
still rule it.
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Around the globe sweeps
a volatile atmosphere...
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and within, a fiery world still burns.
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Floating on this semi-molten interior,
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the plates of the crust
are forever in motion.
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Only in a thin layer between the inner heat
and the atmosphere
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could life arise and thrive...
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yet always at the mercy
of these colossal forces...
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erupting from the depths...
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shaking the solid ground...
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descending from the sky.
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We cannot control such power.
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But we can use our human powers
of invention and discovery--
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to learn, to understand...
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and to survive.
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There are places where primal forces
are still on display,
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where lava streams freely
from the earth's interior.
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Yet these same forces can also
erupt suddenly, unpredictably...
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with terrible consequences.
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For hundreds ofyears,
a volcano called Soufriere Hills
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on the Caribbean island
of Montserrat was dormant.
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But in 1995, some 12,000 islanders
discovered they were living on a time bomb.
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RADlO ANNOUNCERS:
The situation has escalated.
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This followed a major ash fall
atjust after 8:00 this morning.
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The scientists have told us that they can
no longer guarantee six hours notice.
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All incoming data are being processed
on a near real-time basis
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because the volcano can just go off
with little or no warning.
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[siren]
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[rumbling]
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NARRATOR: Deadly cascades ofash, gas,
and lava rocks called pyroclastic flows
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raced down the mountain at temperatures
as hot as 1,000 degrees.
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The eruptions continued, burying
the capital of Plymouth under ash,
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but there was time to evacuate
the population ofabout 4,000...
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and no lives were lost here.
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Yet outside the city,
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pyroclastic flows killed 19 people
who had ignored the warnings.
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Forscientists, this place has become
a kind of living laboratory.
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At the Montserrat Volcano Observatory,
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Dr. Marie Edmonds is part ofa team
from the British Geological Survey.
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EDMONDS: l became a volcanologist
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because we know so little
about these dangerous mountains...
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and l saw that studying them could mean
better forecasts of eruptions,
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which could save many lives.
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l sometimes feel like the volcano
is almost a living thing.
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lt grows, it breathes,
it even has a kind of pulse.
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l grew up wanting to be
an astronaut or a spy--
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but living alongside an active volcano
is just as exciting.
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Right now, there are signs the mountain
is building towards another big event .
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We feel a great weight of responsibility
on ourshoulders.
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But it's difficult trying to figure out
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what might be happening miles below
in the crust of the earth.
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Montserrat is actually the peak
ofan undersea volcano
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which was built up by a collision
between two plates of the earth's crust.
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As the heavier plate plunges
beneath the other,
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intense heat and pressures
melt the leading edge into magma.
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The magma rises into a chamber
and then heads towards the surface.
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lf it reaches the surface quickly,
it can generate enough gas to explode.
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Smaller explosions continued here,
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and during the last couple ofyears
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thick magma has built
a 500-megaton mountain above the vent--
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a huge lava dome.
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We believe it will collapse,
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and that it will trigger more explosions
and potentially dangerous pyroclastic flows.
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NARRATOR The first hint
of danger comes
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when seismic instruments show
increasing swarms ofearthquakes--
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a sign that magma is rising,
causing tremors within the volcano.
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Routine monitoring takes on
a new urgency.
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They need to check the instruments
designed by Marie
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that constantly monitor gases
rising from the volcano.
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EDMONDS: We've discovered that ifthe volcano
suddenly exhales more gas,
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it can mean that the activity
is ramping up to an eruption.
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So today the volume is up,
and that's a worrisome sign.
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Next we have to fly as close as possible
to the crater of the volcano
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to get more data
and to evaluate the situation.
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This is one of those times when
the research we conduct is a bit risky...
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especially for my partner
Richard Herd.
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One of his jobs is to install
a laser reflector,
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which can measure even a few millimeters
of ground deformation.
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That can tell us if magma
is filling the chamber below
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and causing the ground to swell.
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We avoid dangerous situations
unless it's absolutely necessary.
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Too many researchers have died in recent years
because eruptions surprised them.
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NARRATOR: All of the evidence suggests
that the dome is increasingly unstable.
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The collapse seems imminent.
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Warnings from the scientists convince
the government to begin evacuations.
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On a July night, it happens.
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[rumbling]
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Violent eruptions send ash clouds
rocketing ten miles high.
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[people singing Amazing Grace]
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Because of the warnings,
not a single life is lost.
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Ash still falls occasionally, but most
have learned to live with it.
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EDMONDS: Most likely the eruptions
will pause for a while,
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then begin a new eruptive cycle.
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But as long as we continue
to monitor the volcano,
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as long as we continue
to unravel its secrets,
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there's no reason for anyone else on Montserrat
to be harmed or to lose their life...
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and that in itself
is reason for celebration.
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NARRATOR: What scientists
learn in Montserrat
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could help reduce risk for millions of people
living near volcanoes around the world...
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but there is another kind ofevent
caused by forces below
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that is even harder to predict,
and far more dangerous.
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Among the places at greatest risk
is a heavily populated part ofTurkey,
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where shifting plates of Earth's crust
meet along a 1,000-mile seam.
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lt's called the North Anatolian Fault,
and it can produce a sudden catastrophe--
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one of the deadliest
ofall natural disasters--
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an earthquake.
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lfwe could pull the plates apart...
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and descend within...
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we'd see that 10 or 15 miles down
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they begin turning into extremely hot,
putty-like rock,
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sliding in opposite directions
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atop the semi-molten interior
farther below.
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Somewhere along the fault,
the plates lock together,
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and over long periods of time,
enormous pressure builds.
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Eventually they break loose
and rip past one another,
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unleashing powerful waves ofenergy
that race through the crust,
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shaking the surface above.
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[man chanting]
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Nearly atop the fault
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lies one of the world's great cities--
lstanbul, Turkey--
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which has been jolted by earthquakes
across recorded history.
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ln the heart of the city,
one remarkable structure
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has remained standing
through 14 centuries of quakes...
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The Hagia Sophia is an enduring marvel
ofart and architecture.
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But for one man, it's also a treasure-house
of geologic history.
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Geophysicist Dr. Ross Stein
has spent more than a decade
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studying earthquakes in Turkey,
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trying to find ways offorecasting
when and where they will strike.
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Here, he found a critical piece
of the puzzle.
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STElN: When l first learned
that since ancient times,
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the clerics of Hagia Sophia
kept records of their earthquake repairs,
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l was tremendously excited.
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Because with such a chronology
of quake dates and damage--
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combined with other data--
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we might discover a pattern that
could help us forecast quakes.
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Such a discovery is
every scientist's dream.
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And in some ways it came true.
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lt turned out that 11 major quakes
in the last 60 years
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had occurred in a largely
westward progression.
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And l kept asking myselfwhy.
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We went out to take a look
at each quake site,
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and we began to form an idea
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about how built-up stress
where the plates are locked
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suddenly gets moved
during an earthquake.
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We turned our data into a computer model
ofstress being transferred by a quake...
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with red showing where stress
increased along the fault,
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and blue where stress was relieved.
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Suddenly, the puzzle pieces fit together.
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With each quake,
stress didn'tjust dissipate...
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but moved down the fault,
where it concentrated again.
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And in most cases, a major quake struck
in the red zone where stress had increased.
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Our model suggested
the next great quake
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might strike lzmit, a city
of more than 200,000 people.
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NARRATOR: And on August 17, 1999,
disaster did strike.
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The lzmit earthquake was a magnitude 7.4
and lasted 45 seconds--
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an eternity to those
who suffered through it.
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[sirens]
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Local news crews
captured the aftermath,
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as rescuers searched for thousands
of people trapped under the rubble.
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20,000 buildings were destroyed...
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halfa million people left homeless.
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Some believe the death toll
reached as high as 25,000.
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The real toll may never be known.
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The loss of life was caused in large part
by substandard construction.
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ln many places,
cheaply built modern structures
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lay in ruins next to undamaged
ancient mosques.
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STElN: Almost immediately
after the quake hit,
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the international community arrived
with food, medicine and shelters.
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most of the residents
are choosing to rebuild in lzmit,
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but ifthe lessons we've learned here
aren't acted upon,
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their future is not bright.
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The most important thing we can do
is to build safer structures--
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and we know how--
we just have to make it a priority.
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What l want to do
is to improve our ability
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to forecast when and where
an earthquake will strike.
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We calculate that stress has now
reached a segment of the fault
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beneath the Sea of Marmara.
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Sadly, this area where the next
major quake is most likely...
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is just ten miles south of lstanbul,
a vibrant city ofsome 10 million people.
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To give these millions of people a warning
just before a major quake hits,
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seismometers have been placed
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near the fault segment we think
is most likely to rupture.
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Warnings could reach lstanbul
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a mere 10 to 20 seconds
before the violent shaking waves arrive...
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and the hope is that people
will have a few moments
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to get themselves and their families
to a safe spot.
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lt's almost impossible
to convince people
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that they have a serious
earthquake problem to contend with
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unless they get some kind
of dramatic warning sign...
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and for lstanbul,
lzmit was that warning.
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NARRATOR: The earthshaking forces beneath us
interrupt life only occasionally,
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but unfolding constantly above us
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is the clash of great forces
we know as weather.
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00:27:10,170 --> 00:27:15,591
The fluid gases of the atmosphere
can unleash devastating power.
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This is home ofsome of the most
severe storms on Earth,
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a Midwestern region of the United States
known as Tornado Alley.
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ANNOUNCER: Conditions are pretty favorable
forsome explosive thunderstorm development,
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in fact some of that's
going on right now.
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There's going to be a threat
ofsevere thunderstorms, large hail.
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The storms continuing to intensify.
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Take your tornado precautions.
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Do it now.
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[glass breaking]
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[sirens]
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NARRATOR: On May 3, 1999,
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an extraordinary series of tornadoes
ripped through Oklahoma
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00:29:09,789 --> 00:29:13,417
and left behind almost
unimaginable destruction.
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00:29:15,962 --> 00:29:17,796
MAN: As l remember 2x4s snapping.
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They just snapped like toothpicks,
you know?
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00:29:21,760 --> 00:29:23,635
MAN: Everybody says
what do they sound like?
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00:29:23,678 --> 00:29:25,679
lt sounded pretty much
like a freight train.
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But you are underneath the train.
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MAN: The house was gone.
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00:29:29,267 --> 00:29:32,644
And l haven't found
the refrigeratoryet.
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00:29:37,317 --> 00:29:39,067
MAN: l looked out across the street.
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00:29:39,110 --> 00:29:41,195
And l said, there's no houses
across the street.
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00:29:41,237 --> 00:29:44,364
l can see until Fourth Street.
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00:29:56,544 --> 00:29:58,504
NARRATOR: Many survivors
were warned in time
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00:29:58,546 --> 00:30:02,674
thanks in part to an unconventional
team ofscientists.
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00:30:06,554 --> 00:30:11,558
ltwas these Doppler-radar trucks,
venturing close to the 1999 storms,
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that clocked the fastest wind speed
ever recorded near the ground--
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00:30:15,605 --> 00:30:18,690
301 miles per hour.
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00:30:20,777 --> 00:30:26,198
Dr. Joshua Wurman and his team spend
months each year chasing tornadoes,
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00:30:26,241 --> 00:30:30,202
hoping to get a radar's-eye view
inside them.
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00:30:40,171 --> 00:30:41,880
WURMAN: For a long time,
l've dreamed ofsolving
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the biggest mystery
about tornados--
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how they're born.
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my goal is to get
a three-dimensional picture
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of the wind speed and wind direction
within the storm.
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But first, we have to position
our two trucks
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on different sides ofa storm
at roughly a 90-degree angle
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and be in just the right place
as the tornado begins.
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We don't know exactly
how a tornado starts...
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but we do know what precedes it.
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Here, warm moist air
from the Gulf of Mexico
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rushes upwards through cooler air,
forming a thunderstorm.
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00:31:32,682 --> 00:31:38,812
Some of the rising air cools and sinks,
or is dragged down by rain and hail.
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The warm air racing in at the bottom
can actually push on the higherwinds aloft,
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sort of tilting them and forming
a large spinning column.
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Somehow, down near the ground
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between the air rushing up
and the air rushing down,
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the spinning dramatically intensifies.
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The thing that fascinates me
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is that only some storms
spawn tornadoes.
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lfwe could figure out which ones,
we could warn people earlier.
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That's why we drive about
10,000 miles every spring.
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Most of the time
we miss the tornadoes.
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lt's incredibly difficult.
l've been trying foryears.
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MAN: Apparently the weatherservice
is saying this storm
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is capable of producing soft balls--
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that's 4.5-inch hail.
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l don't know if l buy it,
but l thought l'd pass that along.
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NARRATOR: Near the end
of one recent season,
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the team received word that
a violent storm was developing--
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one that might spawn
an outbreak of tornadoes.
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The challenge would be
getting there in time.
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MAN: OK, both cells look pretty good.
Both have hooks on them.
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The western one looks like it has
a better hook on it now.
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NARRATOR: lt's a drill they've
been through many times...
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one fraught with frustrations.
270
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An empty gas tank...
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empty stomachs...
272
00:33:56,200 --> 00:33:58,368
inevitable indigestion....
273
00:34:00,163 --> 00:34:01,830
and unpredictable delays.
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00:34:01,873 --> 00:34:04,666
[train horn blows]
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This day would prove
even more eventful than usual.
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MAN: The shoulders are a bit muddier
than l expected.
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l tried to rock it back and forth
and when it went backwards...
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and is quite stuck.
279
00:34:24,979 --> 00:34:29,066
NARRATOR: The storm
was coming right at them.
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All they had to do
was get unstuck.
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00:34:35,948 --> 00:34:37,991
WURMAN: Rotation is just about
due west of us.
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Still about, l would say,
5 kilometers, maybe 4 1/2.
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Where is the rotation
relative to you?
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MAN: lt's moving directly toward us.
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00:34:53,257 --> 00:34:55,092
There's no reason
to panic on this, right?
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WURMAN: Uh, not yet.
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00:35:01,766 --> 00:35:03,058
[cheering]
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00:35:03,101 --> 00:35:04,518
Are you unstuck?
289
00:35:04,560 --> 00:35:06,978
MAN: Yes, yes, yes, unstuck.
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00:35:10,483 --> 00:35:14,402
WURmAN: OK, we're seeing
increasing rotation at lower levels.
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00:35:14,445 --> 00:35:17,030
Would you concurwith this?
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NARRATOR: Afteryears of near misses,
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00:35:20,409 --> 00:35:24,663
Josh Wurman's team
was in perfect position--
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and this storm was cooperating.
295
00:35:30,878 --> 00:35:32,129
WURMAN: Curtis.
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00:35:32,171 --> 00:35:34,214
CURTlS: Stand By.
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00:35:34,257 --> 00:35:35,799
WURMAN: Curtis.
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00:35:35,842 --> 00:35:38,385
CURTlS: l'm looking at it.
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00:35:38,427 --> 00:35:41,221
We got one now.
We're getting it right now.
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NARRATOR: For the first time ever,
the team succeeded
301
00:36:23,014 --> 00:36:25,265
in recording with two Doppler radars
302
00:36:25,308 --> 00:36:31,354
the conditions within a storm
at the moment the tornado formed.
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00:36:31,397 --> 00:36:33,815
The data will take years to analyze,
304
00:36:33,858 --> 00:36:40,655
but it promises to help unravel the secret
of how this tornado was born.
305
00:36:44,327 --> 00:36:49,039
lt was a victory forscience,
for Josh Wurman and his crew,
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00:36:49,081 --> 00:36:54,336
and for those whose lives will one day
be safer because of their efforts.
307
00:37:03,638 --> 00:37:07,224
WURMAN: As scientists we yearn
to witness the unknown...
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00:37:07,266 --> 00:37:10,602
to see things that have
never been seen before.
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00:37:10,645 --> 00:37:16,358
Hundreds ofyears ago that would have been
new rivers or new islands.
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For me that unknown
is the inside ofa tornado.
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EDMONDS: Working to decipher powerful events
like a volcanic eruption
312
00:37:39,340 --> 00:37:42,217
is really searching for patterns
that will alert us
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00:37:42,260 --> 00:37:44,386
when something terrible
is imminent,
314
00:37:44,428 --> 00:37:48,515
so that every human life at risk
can be saved.
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00:37:48,557 --> 00:37:55,063
Only 19 people died here on Montserrat,
but that's 19 too many.
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00:37:57,483 --> 00:37:59,401
STElN: Several hundred million people
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00:37:59,443 --> 00:38:03,697
live along the world's
most active earthquake fault zones.
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00:38:03,739 --> 00:38:08,368
So it's critical we get better
at forecasting quakes.
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NARRATOR: lfthese and otherscientists
can add a little bit to our understanding,
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00:38:16,961 --> 00:38:20,755
then one day the pieces
will fit together.
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00:38:20,798 --> 00:38:22,590
And we have that power--
322
00:38:22,633 --> 00:38:27,053
to explore, to learn,
to find ways ofsurviving--
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00:38:27,096 --> 00:38:31,599
no matter how powerful
the forces that confront us.
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00:39:29,241 --> 00:39:32,952
ALEX: Seems to be going
northeast now.
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00:39:32,995 --> 00:39:34,329
SEAN: Hey, get me a wide lens--
326
00:39:34,372 --> 00:39:39,042
get me the 40 orsomething.
327
00:39:39,085 --> 00:39:41,252
ALEX: Going increasingly north,
continues at present path,
328
00:39:41,295 --> 00:39:45,507
it will be rounding over
towards us.
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00:39:45,549 --> 00:39:46,800
GREG: 40-millimeter?
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00:39:46,842 --> 00:39:49,260
SEAN: Yeah.
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00:39:51,180 --> 00:39:53,223
[jiggling door handle]
332
00:39:53,265 --> 00:39:56,643
SEAN: Unlock, unlock, unlock.
333
00:39:59,188 --> 00:40:00,814
Open it.
334
00:40:03,692 --> 00:40:06,945
Unlock it! Unlock!
335
00:40:06,987 --> 00:40:08,279
GREG: Locked out?
336
00:40:08,322 --> 00:40:09,989
SEAN: Yeah.
27912
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